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Front. Environ. Sci., 10 May 2022 |

Satellite Analyses Unravel the Multi-Decadal Impact of Dam Management on Tropical Floodplain Vegetation

www.frontiersin.orgLuca Salerno1*, www.frontiersin.orgÁlvaro Moreno-Martínez2, www.frontiersin.orgEmma Izquierdo-Verdiguier3, www.frontiersin.orgNicholas Clinton4, www.frontiersin.orgAnnunziato Siviglia5 and www.frontiersin.orgCarlo Camporeale1
  • 1Department of Environment, Land and Infrastructure Engineering, Politecnico di Torino, Turin, Italy
  • 2Image Processing Laboratory (IPL), Universitat de València, València, Spain
  • 3Institute of Geomatics, University of Natural Resources and Life Science (BOKU), Wien, Austria
  • 4Google, Inc., Mountain View, CA, United States
  • 5Department of Civil, Environmental and Mechanical Engineering, Università degli studi di Trento, Trento, Italy

An assessment of river regulation impact on floodplain vegetation is crucial to developing a modern watershed management approach in the Neotropics aimed at mitigating alterations of the floodplain environment. Floodplain forest monitoring requires high–resolution mapping, as vegetation dynamics are in the narrow area at the interface between terrestrial and aquatic systems. The existing satellite images that afford land observations have limitations due to coarse resolution or gaps in data caused by the extreme cloudiness of tropical regions. This study provides a new framework for high-resolution mapping and monitoring of a large-scale tropical forest in the aquatic-terrestrial zone of an Amazon basin. The main aim is to assess the vegetation status and the environmental degradation in a highly altered fluvial setting. To achieve the goal, a remote sensing processing chain, which couples hydrologic and vegetation data, was developed. A map of high-resolution traditional vegetation indices and their non-linear generalization was derived from the high-resolution gap-free reflectance data obtained by combining Landsat and MODIS data, through the HISTARFM algorithm. Subsequently, hydrological modification within these areas was assessed by using a global water surface dataset. In addition, the impact of river regulation on riverine forest carbon cycling was assessed through the analysis of interannual variability of the gross primary production of floodplain vegetation. The framework was applied to analyze the last 2 decades of changes in the floodplain forest of Uatumã river (central Amazon basin), downstream of the Balbina hydropower dam built in 1987. The analysis showed the presence of vegetation degradation in areas of increased hydrologic stress and upland forest encroachment in areas no longer inundated. The dam continues to have effects on vegetation even 30 years after its construction. The ongoing profound reshuffling of the floodplain forest, and the impact on the carbon storage capacity of the floodplain forest suggest that the situation is far from a new environmental equilibrium. The proposed high–resolution approach allows for a detailed mapping of riparian vegetation alterations, helping to develop a more careful management of the watershed through a better understanding of the human footprint on floodplain forests.

1 Introduction

Floodplain forests represent about 14% of the Amazon Basin area (Flores et al., 2017) and are highly productive riverside areas, heavily influenced by both terrestrial and fluvial dynamics (Junk et al., 1989). The seasonal pattern of precipitation over the Amazon catchments drives a predictable mono-modal annual flood pulse in the unaltered large rivers (Junk et al., 1989; Schöngart and Junk, 2007; Junk et al., 2014).

The natural annual cycle of rising, high, and low water levels, has a strong impact on floodplain forest dynamics acting as a filter that selects a wide variety of flood-adapted species tolerating up to 6–8 months with flooding and up to 10 m of water depth (Junk et al., 1989; Junk, 1997; Lewis et al., 2000; Wittmann et al., 2004; Wittmann et al., 2010). Moreover, the tree endemic species that populate the different topographic levels of floodplains, synchronize their phenology with periodic flood events, water levels, and sedimentation cycles (Worbes, 1997; Junk, 1997; Ferreira et al., 2010; Parolin and Wittmann, 2010; da Rocha et al., 2019).

These complex interactions between water and vegetation life-cycle make the floodplain forests extremely sensitive to hydrological changes due to anthropogenic and natural disturbances. Any kind of alterations in the original hydro-geological drivers can represent a strong stress for riparian species. Long-term negative environmental consequences range from forest degradation, changes in the floristic composition, and reduction of biodiversity, up to the ecological regime shifts in the worst cases (Tockner et al., 2010). Among the anthropic alterations of the riverine environment, the modifications of flood pulse due to hydropower dams may be particularly severe. Many studies have unraveled the impacts of hydroelectric dams (Kahn et al., 2014; Almeida et al., 2019; Kuriqi et al., 2021), highlighting the social, economic and environmental negative repercussions (Nilsson and Berggren, 2000; Fearnside, 2002; Poff and Hart, 2002; Fearnside and Pueyo, 2012; Fearnside, 2014; Castello and Macedo, 2016; Assahira et al., 2017; Cochrane et al., 2017; Timpe and Kaplan, 2017; Agostinho et al., 2018). Furthermore, the consequences of large damming are not only limited nearby the infrastructure, but also affect floodplains downstream and the estuarine environment at large scales (Andersson et al., 2000; Merritt and Wohl, 2006; Tealdi et al., 2011; Castello and Macedo, 2016; Latrubesse et al., 2017). The Amazon basin has a very large number of existing dams 151) with 358 dams planned and under-construction (Zarfl et al., 2015); this makes the amazonian floodplains one of the most threatened ecosystems in the world (Kahn et al., 2014; Lees et al., 2016; de Resende et al., 2020).

The hydroelectric damming may alter the natural flood pulse and disrupt river connectivity (Grill et al., 2019), with serious repercussions on floodplain vegetation (de Resende et al., 2019; da Rocha et al., 2019; Assahira et al., 2017). da Rocha et al. (2019) found that in areas with a drastic reduction of flooding, upland forest species started competing with endemic species by encroaching the floodplains, while in the areas with extreme prolonged flooding the establishment of any species was impeded. Recent studies (Assahira et al., 2017; de Resende et al., 2019) on a regulated river of the Amazonas state (Uatumã) have documented, in the lower lands of the floodplain, a vast mortality of endemic tree species which did not tolerate river flooding lasting several years, associated with the discharge regulation operated by the hydropower dam (Balbina).

Moreover, dams reduce sediment supply causing the rearrangement of the river planform (e.g. reduction of lateral migration (Constantine et al., 2014), channel degradation), inhibiting the rejuvenation process of the riparian vegetation (Camporeale et al., 2013; Vesipa et al., 2017) and promoting vegetation encroachment.

The modification of vegetation species composition, not only jeopardizes several environmental services (de Sousa Lobo et al., 2019), but also may impact the floodplain carbon cycle. In the upper areas of the floodplain, the accumulation of dead biomass is likely to increase the greenhouse gas emissions of these areas. Root mats and litter matter, no longer recruited by floods and bank erosion, remain and increase the vulnerability of areas to fire during droughts (De Almeida et al., 2016; Flores et al., 2017; de Resende et al., 2019).

Moreover, the encroachment of species from the upland forest and the decay of the poorly flood-tolerant species in topographically depressed regions of the floodplain (de Resende et al., 2019; Schöngart et al., 2021) cause a change in gross primary production (GPP) of such areas. These additional impacts on the global carbon cycle, caused by dams, require further investigations and should be added to the budget of known greenhouse gases emissions produced by anaerobic biomass degradation in reservoirs (Kemenes et al., 2011; Deemer et al., 2016; Prairie et al., 2018; Calamita et al., 2021), in order to better assess the carbon footprint of river regulation in the Neotropics.

Although the threats that the large dams represent for the tropical floodplain forest are well known in the literature (Latrubesse et al., 2017), the long-term consequences and the extent of environmental alteration remain only partially understood (Fearnside, 2016). The poor accessibility of tropical floodplains makes field monitoring and measurement campaigns very expensive, challenging and limited to a few spots. In contrast, to better understand and predict the evolution shift of the ecological regime of floodplain forests, an extensive assessment of vegetation is needed. It is crucial to understand if the whole ecosystem resilience is enough for assuring an adaptation to the hydrological changes (Shilpakar et al., 2021) or whether environmental degradation and catastrophic and irreversible shift of the ecosystems are unavoidable (Tockner et al., 2010; Shilpakar et al., 2021). In particular, as the main vegetation dynamics occur in a narrow area, at the interface between terrestrial and aquatic systems, a high spatial and temporal resolution of the data is needed for their analysis.

Remote sensing offers practical and efficient techniques to estimate biochemical and biophysical parameters and to analyze their evolution over time, even for very remote, wide and poorly accessible areas such as tropical floodplains. Although the vegetation index analysis is widely used in floodplain forest monitoring of temperate regions (Sims and Colloff, 2012; Lafage et al., 2014; Nallaperuma and Asaeda, 2020), it is poorly explored in tropical areas where the extreme cloudiness and presence of aerosols do not allow to obtain historical series with adequate spatial and temporal resolution. According to Kobayashi and Dye (2005), the normalized difference vegetation index (NDVI) data from the Advanced Very High–Resolution Radiometer (AVHRR) over the amazonian region show a seasonality mostly caused by variations in atmospheric conditions associated with biomass-burning aerosols and cloudiness. Furthermore, the coarse resolution of NDVI by AVHRR, makes it useless for the analysis of riparian forests. The present study aims to evaluate the impact of dam regulation on floodplain vegetation through a high-resolution satellite-based operative framework. More specifically, we couple temporal evolution analysis of vegetation indices and gross primary production with hydrological transitions data, in order to disentangle the role of river regulation on the floodplain forest alteration. The developed framework was applied to the floodplain of the Uatumã River (Amazonas, Brazil) downstream of the Balbina hydroelectric dam (built in 1987), in order to extensively map the long-term evolution of vegetation in a highly impacted environment due to dam management. Furthermore, the global availability of the adopted datasets makes this analysis potentially applicable to other sites.

2 Material and Methods

Through a remote sensing analysis of satellite data developed on the free-access cloud computing platform Google Earth Engine (GEE) (Gorelick et al., 2017), we have combined forest changes detection with an analysis of the hydrological transitions and the assessment of the annual GPP, in order to assess the impact of dam alteration on floodplain environment in the last 2 decades (2001–2019).

2.1 Study Area

The developed framework was applied to the floodplain of the Uatumã River (Amazonas, Brazil) downstream of the Balbina hydroelectric dam (built in 1987), in order to extensively map the long-term evolution of vegetation in a highly impacted environment due to dam management. The analysis of vegetation focus on changes that occurred during the last 2 decades (2001–2019), while the study of hydrologic alterations involves a period from before the dam has gone into operation until the present (1984–2020).Uatumã river is a left tributary of the Amazon river (the confluence is approximately 270 km NE to Manaus city) and flows through the state of Amazonas (Brazil). The river drains a catchment area of 69,500 km2 of Precambrian geological formation of the Guiana shield (Melack and Hess, 2010) mostly covered by not inundated forest (terra firme) and podzolic white-sand soil. The sediment load is almost absent (Lopes et al., 2019), inducing a river bed stability and slow geomorphic dynamics (Constantine et al., 2014; Junk et al., 2015). The Uatumã is a black-water poorly nutrient river, but it is very rich in humic material derived from the leaching of various compounds from plant biomass and necromass (Myster, 2018), which confer to the water its acidity (pH 4.05 ± 0.2, Targhetta et al. (2015)) and a typical dark coloring. The soil texture of the floodplain is dominated by silt and clay with sand fraction increasing upward (de Sousa Lobo et al., 2019; Schöngart et al., 2021)).

River discharges and water stages have been highly affected by the Balbina hydro-power dam, wich was built between 1983 and 1987. The formation of a vast reservoir, upstream the dam, induced the rapid decay of almost 3,000 km2 submerged forest and the formation of more than 3,500 isolated islands (Benchimol and Peres, 2015; Schöngart et al., 2021). Downstream of the dam, the discharge regulation enforced by the hydropower plant management caused alterations in the hydrological cycle, with several consequences on vegetation, that are not completely understood yet (Fearnside, 1989; de Resende et al., 2019; de Resende et al., 2020).

An increase in the floodplain tree mortality for certain species was documented as early as the first flow regulation during dam construction (1983–1987), with a peak in the first decade of dam operations (1994–1997) (Schöngart et al., 2021). The study region (∼3,000 km2) comprises the Uatumã floodplain downstream of the dam (see Figure 1), including the Uatumã Sustainable Development Reserve (USDR), a protected area that aims to preserve nature, while maintaining and improving the lifes of the population (2100 people) through sustainable development projects.


FIGURE 1. Map of study region. (A) Uatumã river from Balbina Lake to confluence with Amazon river. (B) South America and study region. (C) Study area downstream Balbina dam.

According to the analysis by Assahira et al. (2017), the time series of the unique gauge station that is present downstream of the dam (Cachoeira da Morena, Figure 2), shows that the uninomodal flood pulse pattern—very common in the Amazon basin and characteristic of the Uatumã pre-dam regime—almost completely disappeared after the regulation. The post-dam hydrological regime exhibits a reduction of high-water marks up to 95 cm less (Assahira et al., 2017). Conversely, low water regime during post-dam period experienced an increase in water stages compared to the unregulated conditions (Assahira et al., 2017). We also remark that, since the position of the gauge station is on a terrace, near rapids, the results from its data analysis is expected to underestimate the actual hydrological change induced by the dam (de Resende et al., 2019).

2.2 Satellite Data

Since the vegetation affected by river dynamics populates a narrow area at the interface between the terrestrial and aquatic system, high spatial resolution data are necessary for mapping and monitoring. Landsat-like optical data at 30 m spatial resolution are suitable for the detection of specific changes in land cover. Nevertheless, the extreme cloudiness of the Neotropics adversely affects the optical satellite land surface observations.

To obtain gap-filled high spatial resolution reflectance data, Landsat surface reflectance data with a temporal resolution of 16 days and 30 m spatial resolution, and daily MODIS acquisitions at 500 m were combined by the HISTARFM algorithm. The algorithm was implemented by Moreno-Martínez et al. (2020) on the GEE cloud computing platform. HISTARFM filters out random noise and reduces the bias of Landsat spectral reflectances based on Bayesian estimations and Kalman filter. The former estimates the Landsat reflectance values for a given time by combining historical Landsat time series and MODIS and Landsat fused values. The latter corrects the bias of the reflectance product by the previous estimation (for further information, see Moreno-Martínez et al. (2020)).

In this way, gap-filled reflectance data (GFHR) at 30 m spatial resolution was generated from 2001 to 2019 over the whole study area. Then, the high–resolution products of the normalized difference vegetation index (NDVI), its nonlinear version (kNDVI), and the enhanced vegetation index (EVI), were derived from the GFHR data. The indices NDVI and EVI have been widely and commonly adopted in satellite-based vegetation monitoring. In particular, NDVI has been considered an indicator of photosynthetic activity (Weier and Herring, 2000) whereas the EVI is optimized for high biomass regions and mainly focuses on the canopy structure and is less sensitive to atmospheric alterations (Huete et al., 2002). The kNDVI has been recently proposed as a novel alternative to NDVI that improves the performance with respect to saturation, bias, and complex phenological cycles (Camps-Valls et al., 2021). Formal spectral definitions of the three indices are reported in the Supplementary Material.

2.3 Data Masking

A mask for the water bodies was generated to exclude from the analysis the areas perennially flooded and to avoid misclassification in vegetation changes. The Modified Normalized Difference Water Index (MNDWI) calculated from the GFHR temporal series was used in an unsupervised classification approach, consisting of the Canny edge filter and the Otsu thresholding (Donchyts et al., 2016) in order to obtain the optimum threshold.

Monthly water surface maps between 2001 and 2019 were obtained through the classification of GFHR data. The pixel probability of water presence was obtained for all the pixels of GFHR temporal series. The probability was calculated by dividing the number of water occurrences in the temporal series by the total number of years. Pixels with a water probability value higher than 0.8 (i.e. 80%) were excluded from the vegetation change detection. Further details on the identification of areas with vegetation loss or gain are provided in the Supplementary Presentation (section Identification of Regions of Interest).

2.4 Vegetation Change Detection

The time series of each index was analyzed separately, through a set of segmentation algorithms (LandTrendR, see Kennedy et al. (2018)). The algorithms aim to identify breakpoints in the time series separating periods of durable changes or stability in temporal evolution of the vegetation index. The results of segmentation provide a simplified representation of index history of a pixel as segment lines whose vertex are the breakpoints, identified by year and spectral index value (details are reported in Kennedy et al. (2018) and are recalled in Supplementary Figure S1 of the Supplementary Material). Since the algorithms require that the input collection must include only one observation per year, monthly GFHR-based vegetation maps were used to derive the time series of the median annual vegetation index for each pixel. The segmentation process was set up to exclude vegetation changes with a recovery time of 1 year, which are not consistent with vegetation dynamics and are likely due to noise. Moreover, a maximum number of six segments was imposed to avoid excessive fragmentation of the time series. The possible identified variations were either a loss or a gain of vegetation. These variations were further filtered so that when more than one change of the same type (loss/gain) was detected in the same pixel only the greatest was reported, indicating the year that changes occurred and its magnitude.

2.5 Assessment of the Gross Primary Production (GPP)

To assess the impact of vegetation alteration on the carbon storage of the fluvial corridor, the inter-annual variability of gross primary production was analyzed. The annual GPP was assessed through a Vegetation Photosynthesis Model (VPM) optimized for broad-leaf seasonally moist tropical evergreen forest, proposed by Xiao et al. (2005). The model divides forest canopy into photosynthetically active vegetation and non-photosynthetically active vegetation. GPP is expressed as


where PAR is the photosynthetically active radiation [MJ/m2], FAPAR is the fraction of radiation absorbed by chloroplasts (photosynthetically active part of vegetation), ϵ0 is the maximum light use efficiency [kg C/MJ] and Wf, Tf, Pf are downregulating stress factors of water, temperature and phenology for light use efficiency, respectively. Following Xiao et al. (2005) the FAPAR is approximated as


and the effect of air temperature on the optical energy utilization is


where Tmin, Tmin, Topt are the minimum, maximum and optimal temperature for photosynthesis, respectively. For tropical conditions they are assumed to be equal to 2 , 48 and 28 °C (Xiao et al., 2005).

The water stress factor Wf depends on soil moisture and/or vapor pressure deficit, and has been derived through a simple approach using the Land Surface Water Index (LSWI, see Supplementary Material and Xiao et al. (2004b,a, 2005))


with LSWImax being the maximum LSWI during the growing season for each pixel.

The role of phenological stress factor, accounting for the influence of leaf age on photosynthesis at canopy level, can be neglected as a first approximation (i.e., Pf = 1), since the canopy of evergreen broadleaf tropical forest is composed of green leaves at various ages (Xiao et al., 2005). GPP was assessed at hourly time step and then cumulated in order to obtain annual values. The procedure for the parameter estimation of the VPM model is reported in the Supplementary Material.

2.6 Region of Interest Analysis

The fundamental unit of this analysis was the Region of Interest (ROI, for definition and further detail refer to Supplementary Presentation). Every ROI was analyzed in order to investigate the nature of vegetation change, the impact on GPP, and any alterations of hydrological status (Figure 3). To describe the evolution of a vegetation index within a ROI over the whole considered time period, a series of monthly representative values of the vegetation index was assessed by spatially aggregating the GFHR-based map within the ROI’s domain. Two sub-series were divided—from 2001 to the yC (i.e., the year in which the change occurred) and from yC to 2019—in order to analyze the response of the vegetation to the change itself. To detect a trend in the sub-series, a linear regression analysis of the smoothed data (with a 6-months centered moving average) was performed. The average amplitude of oscillations of both sub-series was defined as the mean of the absolute difference between the original signal and its moving average.

Due to the paucity of hydrologic data to perform a statistically robust analysis of the impacts of the dam on the floodplain, we adopted a remote sensing approach. The hydrological alterations that occurred in Uatumã floodplain during the last 3 decades were assessed through the analysis of the Global Water Surface dataset (Pekel et al., 2016). This dataset maps the location and the temporal distribution of surface water from 1984 to 2020, thus allowing to follow water surface behavior from just before the end of the dam construction to the present day. More specifically, each ROI was characterized through the information on change in seasonality (i.e. change in intra-annual behavior of water surfaces) between the 1984 and 2020, as provided by the dataset. The dataset, in fact, reports changes between the three classes of not-water, seasonal water, and permanent water and it therefore allows for the identification of a hydrology-induced shift in the flooding regime that occurred in the ROI.

The effects of the vegetation changes on the carbon cycle were evaluated through the analysis of the annual spatial distribution of GPP. In each ROI, the annual time series of the spatial median (GPPm(t)) and the variance (GPPσ(t)) was calculated and analyzed (see Supplementary Material) in order to detect trends in both parameters.

3 Results

In this section we present the results obtained with each of the three vegetation indices: kNDVI, NDVI and EVI. The results will be shown separately, and hereinafter, they will be reported with a triplet of values, using the same order.

The total area of detected vegetation loss was 53.70, 27.60 and 13.23 km2 (Table 1). The kNDVI was the most sensitive index in vegetation loss detection with area and number of ROIs nearly double and quadruple the one identified by NDVI and EVI (Table 1). The area of vegetation loss common to all the three indices was 11.36 km2 and represents the 86% of EVI-based detected forest loss.


TABLE 1. Spatial extension of loss and gain with the three indices. The asterisk refers to the percentage of ROIs’ total area with a hydrologic change.

3.1 Vegetation Changes

Vegetation loss that occurred during the first decade of the analysis period (2001–2010) accounts for 61, 69, and 69% of the totality, with most of this due to a gradual decreasing of the vegetation index (see Figure 4). During the second decade (2011–2019) the loss was concentrated in the year 2015 (Figure 4). This peak coincides with the occurrence of a severe drought induced by ENSO oscillations (2015–2016) that affected especially the higher elevations of the region. Furthermore, the highest lands are rich in the sandy fraction (Schöngart et al., 2021), implying less water retention. The disappearance of the flooding in those zones, a lowering in the rainfall and in water table increase the severity of drought periods (Parolin and Wittmann, 2010). The distribution of (normalized) change in the vegetation index for the ROIs with a loss is bell-shaped, with the mean, median, and mode values very close to each other (see Figure 5).


FIGURE 2. Water levels in gauge station Cachoeira Morena.


FIGURE 3. Flowchart of the framework used for the vegetation analysis. (1) Moreno-Martínez et al. (2020), (2) Donchyts et al. (2016) (3) Robinson et al. (2017), (4) Xiao et al. (2005), (5) Pekel et al. (2016).


FIGURE 4. Distribution of the year of change. The blue-dashed portion of the distributions refers to the subset of ROIs wherein an hydrological alteration also occurred. (A)(C) distributions of the year of change for the ROIs with a vegetation loss detected through kNDVI, NDVI and EVI, respectively. (D)(F) distributions of the year change for the ROIs with a vegetation gain detected through kNDVI, NDVI and EVI respectively. It is conventionally assumed that all changes caused by a monotonous increase or decrease in the vegetation index occurred in the first year of the analysis (yC = 2001).

Concerning the ROIs in the floodplain performing a vegetation gain, they involve a surface much larger than the ROIs with a loss. The interested area of vegetation gain amounts to 109.63, 63.72, 62.71 km2, as detected by kNDVI, NDVI or EVI, respectively (Table 1). The overall area for vegetation gain commonly detected by all the indices is 41.16 km2 (amounting to 65% of the area detected by EVI). The vegetation gain is mainly comprised by gradual monotonous increase in the index (72, 82 and 82% of the overall gain, see Figure 4), and this was due to natural tree growth. It was conventionally assumed that all monotonic increases or decreases in the vegetation index occurred in the first year of analysis (yC = 2001, see Figure 4).

The reduction in the oscillation amplitude occurred after the year of change yC for the majority of the ROIs having a vegetation gain (specifically, 71, 84, 91%, see Figures 6D–F). This suggests a change in the phenology and/or a change in species populating the floodplain in favor of a terrestrialization of the forest community. In contrast, loss of vegetation is markedly associated to an increase in the oscillation amplitude (65, 67, 77%, see Figure 6A–C).


FIGURE 5. Distribution of the (ROI-averaged) magnitude of (normalized) change. The top panel explains how this quantity has been evaluated for a single pixel. Distributions in (A)(F) refer to spatial mean values of the magnitude within each ROI. The blue-dashed portion of the distributions refers to the subset of ROIs wherein an hydrological alteration also occurred. (A)(C) refer to the ROIs with a loss whereas (D)(F) refer to ROIs with a gain. Features of the distributions are reported in the boxes.

The linear regression of the vegetation index time series shows a positive trend, after the change, for more than 95% of ROI with a gain (Figures 7D–F). This indicates that the increase in the index did not stop after the year of the change but is still in progress. On the other hand, for nearly 60% of areas with a vegetation loss, a slight recovery followed after the change (Figures 7A–C). Such trends, along with the increase in the oscillation amplitude are probably due to the growth of grassy-like species. Furthermore, for 40% of ROIs with a vegetation loss the index continued to decline after the year of change, thus suggesting a decay towards an unvegetated condition (Figures 7A–C).


FIGURE 6. Distribution of the (ROI-averaged) relative difference in the amplitude of intra-annual oscillation of the vegetation index, before and after the change within ROIs. The top panel explains how this quantity has been evaluated for a single pixel. (A)(C) Forest loss (D)(F) Forest gain.

3.2 Hydrological Changes

The global map of the water surface developed by Pekel et al. (2016) provides precious information about the spatio-temporal distribution of water surface of the last 3 decades, with related statistics. Furthermore, Pekel et al. (2016) developed a map capturing the transitions in the hydrological behavior. More specifically, Pekel et al. (2016) identified eight transition classes of change in seasonality (see definition in the caption of Figure 8) between the three classes of not water, seasonal water, and permanent water (see the original paper for further details about the transition classes). The datasets are annually updated, and the current version (v.1.3) analyzes the global water surface from 1984 to 2020. In the study area of the Uatumã river, about 164 km2 of permanent water and about 23 km2 of seasonal water remained so after the dam construction. On the contrary about 29 km2 of land spots and 5.9 km2 of permanent water shifted to seasonal waters after the discharge regulation operated by the dam. Finally, a wide area of floodplain was no longer affected by seasonal floods: about 5.4 km2 shifted to totally terrestrial behaviour, while 33.5 km2 experienced only a period of seasonal flooding after dam construction and subsequently came back to terrestrial lands.


FIGURE 7. Distribution of the (ROI-averaged) slope of the linear regression of the index time series within ROIs after year of change. The top panel explains how this quantity has been evaluated for a single pixel. (A)(C) Forest loss (D)(F) Forest gain. The vegetation changes are detected through kNDVI ((A),(D)), NDVI ((B),(E)) and EVI((C),(F)).

3.3 Hydrological Impact on Vegetation

By comparison of water transition maps with the above results, we were able to identify the hydrological transitions that occurred within the ROIs after dam construction. The results show that vegetation loss or gain are affected by different kinds of hydrological alterations (see Supplementary Figure S10). The 60, 64, 48% of loss (Figure 5 and Table 1) occurred in areas interested by river dynamics, namely areas flooded quite regularly. More than half of these areas (53.8, 55.8, 61.5%) consist of land areas in which a seasonal flooding regime has been established after dam construction (Supplementary Figure S9A,C, transition class E). Nearly one-fifth (specifically, 19.8, 14.5, 22.9%) of such a hydrologically-induced vegetation loss occurred in areas where an ephemeral seasonal regime was established and subsequently disappeared (Supplementary Figure S9A,C, transition class J). The remaining vegetation loss occurred in areas that remained permanently or seasonally inundated despite of dam regulation (Supplementary Figure S9A,C, transition classes A and D).

As shown in Figures 5A–C, the vegetation loss that occurred in areas interested by river dynamics (see blue-dashed bars) represents almost 70% of high-magnitude vegetation changes (i.e., magnitude values higher than the mode). The remaining 30% can be partly due to anthropic use (forest logging, agriculture use, etc.) of the floodplain permitted in the Uatumã Sustainable Development Reserve by the Brazilian authority (Schöngart et al., 2021). On the contrary, the area of forest loss characterized by low-magnitude changes (smaller than the mode) but unrelated to the hydrological regime is respectively 45, 40 and 67% (Figures 5A–C). Since, in this latter case, the ROIs are far from the active channel (see Figure 8), and given the low magnitude of the changes, that vegetation alteration may be caused by temporary vegetation stress not directly related with dam regulation. After comparing the distributions of the magnitude of vegetation gain of all ROIs with the ones interested by river dynamics (Figures 5D–F), it is markedly evident that the forest gain is localized in areas that have undergone an hydrological alteration (regardless of the magnitude of the changes and the index adopted). About 80, 89 and 84% of the total vegetation gain occurred in fluvially-affected areas (see Table 1 and Figures 5A,C). In particular, most of them occurred in land spots shifted to seasonal waters after the dam construction and that subsequently came back to terrestrial lands (Supplementary Figure S10D-F class J).

3.4 Changes in the Gross Primary Production

The forest changes induced by the Balbina dam construction have generated a complex vegetation redistribution of the Uatumã floodplain. Some areas shifted to unvegetated conditions while others underwent a modification in the structure of the plant community. Such a redistribution may alter the capability of the floodplain forest to store carbon, thus affecting the river carbon cycle. For this purpose, high-resolution (30 m-pixel) annual GPP maps were developed through the VPM model (Xiao et al., 2005) (Figure 9). In the present study, the impact of river regulation on the forest carbon cycle was assessed through the analysis of the GPP trajectories within each ROI. The annual spatial variance of GPP was used as a proxy of land cover heterogeneity while the temporal changes in the GPP were assessed by monitoring the spatial median of the annual values (see Supplementary Material). Four combinations of changes are therefore possible for both the vegetation loss and gain conditions, depending on the increase/decrease of the spatial variance/median of GPP annual values, respectively (see Figure 10). For example, in 52.7% of ROIs detected by the kNDVI (see Figure 10A) a vegetation loss is characterized by a decrease in the mean GPP and an increase in the variance. This means that those ROIs, after the change, underwent an increase in the cover heterogeneity (e.g., with a patchy pattern) but a reduced overall gross primary production.


FIGURE 8. Alteration in the hydrological conditions of study area. a-c Frequency of water presence from 1984 to 2020. d-f  Maps of hydrological transition occurred between 1984 and 2020; (A): unchanging permanent water surfaces; (B): new permanent water surfaces (conversion of land into permanent water); (C): lost permanent water surfaces (conversion of permanent water into land); (D): unchanging seasonal water surfaces; (E): new seasonal water surfaces (conversion of land into seasonal water); F: loss of seasonal water surfaces (conversion of a seasonal water into land); (G): the conversion of seasonal water into permanent water; (H): conversion of permanent water into seasonal water; (I): ephemeral permanent water (land replaced by permanent water that subsequently disappears) J: ephemeral seasonal water (land replaced by seasonal water that subsequently disappears). For further details about frequency of water presence and definition of hydrological transition classes refer to Pekel et al. (2016). (G-I) ROIs with a vegetation gain detected by using NDVI index. (J-L) ROIs with a vegetation loss detected by using NDVI index. For graphical reasons, only the some reaches of the area of study are here reported. The whole region and results of all vegetation indices are reported in the Supplementary Figure S3-S8.


FIGURE 9. Comparison between annual gross primary production maps (30 m resolution) of Uatumã floodplain forest in 2001 (A) and 2019 (B). (C) and (D) detail of river stretch (red box) affected by greatest changes in GPP in 2001 and 2019 respectively.

More generally, the results reported in Figure 10 show how the ROIs characterized by a vegetation loss were largely associated to a reduction of GPP in the period 2001–2019 (see Figures 10A–C, further details are in the Supplementary Material). About a third of these cases are associated with a decrease in the heterogeneity of the land cover within the ROI, which could indicate bare soil formation or uniformly distributed vegetated areas with low GPP (e.g. grassland). The remaining two-thirds experienced an increase in land heterogeneity, suggesting a vegetation loss with a leopard-spot pattern. A considerable amount of forest gain (82, 89 and 77%) was associated to an increase in both the median value of GPP and land cover heterogeneity (Figures 10D–F). According to the field survey made by da Rocha et al. (2019), it is reasonable to suppose that this is due to the encroachment of land forest species in the floodplain forest.

The increase in the heterogeneity suggests a shifting condition, with a patchy distribution, that is far from a stable mature forest. Nevertheless, in at least 17, 25 and 28% of cases, a first increase followed by a decrease in the variance may suggest that the change is in an advanced state, because a first reorganization of the community structure (increase in heterogeneity) was followed by a homogenization of the patch (Supplementary Figure S1). Although the behavior of GPP spatially-average values within the entire river corridor is similar to that of the adjacent forest, the analysis of the ROIs shows a different story. Some large areas are overcoming an increase in GPP, while others a decrease in primary production. More specifically, the greatest changes are concentrated in a stretch of floodplain about 45 km long, that is 50 km from the dam (see red box Figure 9), where the presence of ROIs and hydrological alterations are concentrated.

4 Discussion

4.1 The Framework

The framework proposed in this study aims to assess the alterations in a tropical floodplain forest induced by river regulation due to damming. The main outcomes of the present approach are the: 1) detection and characterization, through a high-resolution analysis, of vegetation changes, in terms of phenology, trajectory of the change, and GPP estimation and the 2) identification of the relation of the changes detected with the local alteration in the hydrologic regime.

The vegetation analysis is based on four pivotal aspects: 1) The analysis of the floodplains with a resolution consistent with the scales of the process; 2) The adoption of different vegetation indices in order to capture the wider range of vegetation alteration states in a robust way; 3) The development of monthly gap-free land observations along the whole study period that allows obtaining information about the vegetation phenology; 4) Identification of the site where vegetation change occurs and their analysis at the site-scale in contrast to floodplain-averaged lumped analysis, as previously made in the literature. The high resolution of reflectance dataset has a crucial role in detecting the changes that interested the narrow aquatic-terrestrial transitional zone. In the considered case, our estimates from the comparison between the maximum extension of flooding and the median width of the river active channel in the last 3 decades (through global water surface dataset) show that river dynamics involve about 600 m of the floodplain width. The effects of dam regulation on vegetation are mostly concentrated in this riparian belt, therefore it deserves to be scrutinized with adequate resolution. Although monitoring approaches based on moderate spatial resolution data (e.g. MODIS Zhang et al. (2003)) can compensate the issue of cloud-induced gaps with a high temporal resolution, they provide a too low spatial resolution in the riparian area (1 or two pixels per active riparian width). The GFHR data, used herein, instead provides a much higher resolution (about 20 pixels per width of the riparian belt) allowing for precise identification of the areas affected by vegetation changes (see Figure 8).

de Resende et al. (2019) developed a high–resolution mapping of dead trees in the Uatumã floodplain through segmentation and a supervised random forest classification of radar data. The use of vegetation indices in our approach provides an additional assessment of forest degradation by analyzing a wider range of states of vegetation stress and progressive deterioration (reduction of photosynthetic activity, decrease of forest greenness, etc.). Moreover, GFHR data allows us to analyze a longer period of time than data from radar missions. In addition, the present framework also identifies vegetation gain. In the present case, this allowed us to quantify the invasion of upland forest vegetation throughout the floodplain, which was indeed observed through field measurements in some plots (da Rocha et al., 2019; de Sousa Lobo et al., 2019).

Many of the current vegetation indices based on high-resolution monitoring systems of Amazonian forest (e.g. PRODES-INPE) are constrained to the availability of reflectance data during the annual free-cloud period (July to September) (Shimabukuro and Ponzoni, 2018). Since the data always refer to the same season of the year (only three or 4 months of dry period), it is not possible to evaluate changes in intra-annual behavior and therefore in the phenology of forest species. These approaches aimed to detect deforestation (clearings accumulated up to the previous year) focusing on changes between forest and non-forest status, i.e. vegetation that is not characterized by a forest structure (Shimabukuro and Ponzoni, 2018). Therefore they are poorly suited to monitoring changes in plant species or identifying stress conditions in the vegetation.

In our study, the use of HISTARFM fusing algorithm allows the availability of year-round gap-free data and furthermore to analyze vegetation phenology changes. This is very important in interpreting the type of vegetation change that has occurred. Figure 6 shows that vegetation loss and gain are widely associated with phenology. In the case of a vegetation loss, an increase in the amplitude of oscillation associated with a sharp decrease in the average value suggests that, after the change, grassy or shrub species have settled in the ROI. On the other hand, in the case of vegetation gain, a phenology behavior similar to that of the nearby land forest was often found, suggesting an invasion of this type of vegetation in the floodplain area.

The ROI-scale analysis clearly identifies the location where severe forest reshuffling occurred. On the contrary, a spatially averaged lumped analysis along the whole floodplain may not completely identify the actual modification of the forest, since vegetation losses and gains might compensate each other. Although there are many studies concerning the impact of damming that are based on an average-scale analysis of the entire floodplain, those studies usually aim to evaluate the morphological alterations Nallaperuma and Asaeda (2020), and cannot assess whether a reorganization of the plant community is taking place in the floodplain. Therefore, those approaches risk underestimating the environmental impact in the area. It is possible to see this effect also by observing what we obtained from the analysis of the GPP trajectories. Although the averaged analysis over the whole floodplain does not show significant GPP changes compared to what has been observed in the nearby forest, a detailed analysis of the individual ROI shows that profound changes are occurring within the floodplains (see Figures 9, 10).

The assessment of the hydrological alterations, based on the Global Water Surface dataset from 1984 to 2020 enabled us to perform a large-scale analysis of the floodplain. The 37 years of data made it possible to go back to pre-dam conditions, and thus investigate the consequences of the dam-induced changes in the hydrologic regime on the evolution of the vegetation during the last 20 years. Since the dataset provides data at a global scale, the analysis of hydrological alteration can also be performed upon others non-instrumented watercourses for which insufficient flow data is available. More specifically, the analysis is well suited to detect the wide variations of the flooded area caused by the alterations of natural flood pulse in the unconfined fluvial systems of the Amazon basin.

4.2 Strength and Weaknesses of the Procedure

The proposed framework is exportable to other different locations. It is based on the processing of satellite products freely available on GEE (Landsat, MODIS, ERA5-Land, Global water Surface) and does not require special calibration. Moreover, it is completely implemented on GEE, thus significantly reducing computational cost and storage space.

Although the HISTARFM algorithm showed remarkable efficiency in removing gaps and noise from the signal, the extreme cloud contamination of the Amazonian area cause the presence of residual artifacts. This is due to a non-perfect identification of clouds and their shadows, the paucity of uncontaminated data, and the presence of noise–induced by water (Moreno-Martí nez et al., 2020). To reduce the impact of such artifacts on the floodplain analysis, a post-processing filtering operation on vegetation index time series was performed, and all the unrealistic oscillations were removed.

The threshold used for the definition of vegetation loss/gain is the result of an iterative visual inspection and comparison between the map of changes and high-resolution GEE images. Nevertheless, this choice can be further refined through future field validations. The results of the vegetation change detection show differences, depending on the index adopted. The use of three different indices has the purpose of capturing the widest possible range of alterations in the vegetation (photosynthetic activity, structure of the canopy vegetation density of which the indices are proxies). Although, 70% of the areas of change detected with the EVI were also detected by the other two indices, the kNDVI identifies wider additional areas. Further analysis and comparison with field data are needed to define whether this discrepancy is due to the non–linearity of the index (see Supplementary Material) and the definition of the threshold value for change detection or its sensitivity to particular types of alterations not found with EVI and NDVI.

Since the framework is fundamentally based on the reflectance data of the HISTARFM algorithm, the time interval analysis is linked to the availability of MODIS data, namely after 2000.

The annual high–resolution GPP maps were developed through a VPM model (Xiao et al., 2005). Although the model was designed for broad-leaf seasonally moist tropical evergreen forest, it was used to assess the GPP also in flooded spots wherein vegetation is subjected to complex interactions with river dynamics. The sedimentary processes involved and the hydrologic regime induce different responses for different species, thus giving rise to an extremely complex scenario. During the dry period, some species of floodplain forest experience an increase in the rate of CO2 assimilation due to new flushed leaves (more photosynthetically efficient) and soil aeration (Schöngart et al., 2002; Fonseca et al., 2019; Green et al., 2020). Instead, during long floods, the metabolic activities are reduced to a minimum up to a dormancy status as a survival strategy (Fonseca et al., 2019). However, several studies show that other species (Schöngart et al., 2002) (e.g., evergreen trees in igapó forest) does not completely arrest physiological processes during flooding but they either remain photosynthetically active or flush new leaves and produce flowers and fruits taking energy from carbohydrate reserves through anaerobic metabolism (Schöngart et al., 2002; Schöngart et al., 2005). Generally speaking, even though different species act in a different way to survive a long period of flood due to the reduction of oxygen in the soil, they reduce or completely stop the GPP. This justifies the choice, as a first approximation, to consider null the GPP in the flooded spots for flood events longer than a month. Nevertheless, the maximum light use efficiency of the flooded forest during the dry period was assumed equal to the one of the land forest. This choice is justified because, the purpose of the work is not to calculate the precise amount of the GPP in each point, but to evaluate its trajectory over time in order to detect the changes. Nevertheless, a future calibration of the model with field data might enhance the GPP accuracy.

4.3 Floodplain Alteration

We used Uatumã river as a case study of an altered basin. The construction of the Balbina dam caused a dramatic change in the river hydrological regime. As shown in Figure 2, in the period before the discharge regulation (before 1984) the river was characterized by monomodal flood pulse typical of Amazonian basins (Junk et al., 1989; Junk et al., 2011; Assahira et al., 2017). Our results show that the dam has induced perturbation in the seasonal flooding regime with consequences along the whole floodplain. About 33.5 km2 experienced a seasonal regime only for limited periods and subsequently returned to a terrestrial behavior, 5.4 km2 of seasonal flooded area was no longer interested by river dynamics, while 5.9 km2 of permanent water has became seasonal. According to Assahira et al. (2017), the decrease in the maximum water levels (∼ 95 cm, according to the hydrometric station of Cachoeira da Morena) and the increase in the minimum water levels (∼ 104 cm) caused a massive reduction of area potentially suitable for the growth and survival of typical floodplain forest species. The results show that about 150 km2 of the floodplain forest downstream of the dam has undergone vegetation modification over the past 2 decades. By analyzing changes in vegetation between 2001 and 2019 and also quantifying different forms of vegetation degradation, we found a larger vegetation loss than that one reported by de Resende et al. (2019) for the period 2006–2011. A wide area of highly-degraded vegetation was detected (about 32 km2, with kNDVI), whose 60% shows evidence of vegetation that is stressed or was partially replaced by grassy species, while about 40% shifted toward unvegetated conditions (Figure 7). These changes mainly interested the areas with an alteration of magnitude or flooding frequency.


FIGURE 10. Percentage distribution of combinations of increase/decrease in the GPP spatial median/variance within the ROIs. (A)(C) Rois with vegetation loss. (D)(F) Rois with vegetation gain.

Despite the high tolerance to flooding, igapó forest species are very sensitive to alterations in the flood pulse. The Balbina dam has modified the monomodal alternation of wet/dry periods which characterized the pre-dam natural conditions, thus inducing an increase in low-water regimes and a reduction in high-water flows (Assahira et al., 2017). The extremely long flooding period and the loss in the terrestrial period that characterized some areas of the lower lands (up to 300 days per year of wet conditions) have induced a selection of a limited number of species able to adapt to this regime (de Resende et al., 2019; Schöngart et al., 2021). Some areas experienced a new flooding condition from 2000 without interruption for more than 8 years, inducing massive mortality of M. acaciifolium, one of the most common species in igapó (Assahira et al., 2017; Schöngart et al., 2021). In addition, the peak of forest loss observed in 2005 (Figure 4), coincident with a severe drought following a Niño event, highlights how the dam amplifies the effects of natural disturbances.

The consequences of the hydrological changes are not limited to tree mortality induced by the anoxic conditions of long flooded areas (de Resende et al., 2019), but also include the redistribution of plant species (da Rocha et al., 2019). The suppression of high flow conditions reduces the amplitude of oscillation of the water stage, preventing the floods from reaching the highest elevations of the floodplain (Assahira et al., 2017). The lack of a seasonal inundation at the highest elevations prevents the selection of flood-adapted species and allows for the colonization of invasive species from land forests, and therefore the disappearance of the igapó community (Assahira et al., 2017; de Sousa Lobo et al., 2019; da Rocha et al., 2019). Our analysis of vegetation changes and phonological modifications shows that almost 77 km2 of the floodplain (Figure 6D and Table 1) have undergone a vegetation gain that can be partly associated to a progressive transition from igapó to upland or secondary forest. Although this ecological transition is accompanied by an increase in GPP (Figure 10), it causes a reduction in biodiversity and a modification in ecosystem functioning (de Sousa Lobo et al., 2019; da Rocha et al., 2019), which is a threat to several environmental services (de Sousa Lobo et al., 2019).

In addition, the disappearance of flooding from the upper floodplain partially or completely inhibits the exchange of organic matter and nutrients between the river and the land and worsens the effect of drought events, making the area vulnerable to wildfire (de Resende et al., 2019).

4.4 Multi-Decadal Effects of the Dam on the Forest: A System Still far From Ecological Equilibrium

The Igapó floodplain forest is particularly sensitive to both natural and human-induced changes in hydrology (de Resende et al., 2020). Nevertheless, recent studies using modern radiocarbon techniques have observed that the mortality of some igapó vegetation species in the case of Uatumã mainly occurred after the construction of the dam, while in undisturbed environments it occurred at various times, often associated with La Niña years (de Resende et al., 2019). Our results show that such a vegetation loss downstream of the Balbina dam is still ongoing after 30 years after the construction and does not seem to show a reversal of the trend. Moreover, the floodplain forest is also threatened by species invasion from the land forest.

Damming caused a complex entanglement of terrestrial phase suppression in the lower floodplain region, increasing the alternation between water deficit and anoxic conditions, and the suppression of the aquatic phase in the upper floodplain region. The effects of these disturbances are manifold and still not fully understood. According to Schöngart et al. (2021) the consequences range from the reduction of biodiversity with a loss of ecosystem services, to the increase of greenhouses gasses. Since the high-flow conditions are inhibited, the dead trees remain in the lower part of the floodplain and are exposed to decomposition. The estimates provided by de Resende et al. (2019) predicted that 354 GgC could be potentially emitted from the degradation of dead vegetation downstream of the dam. In addition, a lack of carbon sequestration by vegetation in the remaining unvegetated or highly degraded areas should be considered. Our results show that about 47 km2 of floodplain experienced a decrease in GPP in the last 2 decades. Finally, in the upper regions of the floodplain, emissions from the degradation of root mats and litter, no longer recruited by flooding and levee erosion, and emissions from wildfires represent other sources of greenhouse gases caused by the dam. All these additional emissions worsen the still very high levels of emissions attributed to the dam. The total amount of CH4 and CO2 released from the decomposition of vegetation in the upstream reservoirs, from turbines, and from diffuse sources in the water immediately downstream of the dams, is 2.9 MgC-eq per MWh of energy generated, almost ten times that of the coal-fired thermal power plant (Kemenes et al., 2011).

The Uatumã floodplain forest is also threatened by progressive land forest encroachment. Our study shows that an area of approximately 77 km2 has experienced a progressive increase in the land forest encroachment over the past 2 decades (Table 1 and Figure 4). However, it is unclear whether the hydrological conditions imposed by the dam will lead to a new equilibrium in which the igapó forest will be confined to the boundaries imposed by the dam itself, or whether this ecosystem is doomed to degradation with catastrophic and irreversible shifts of the ecosystem (Tockner et al., 2010; Bertagni et al., 2018). Our analysis of the GPP trajectory shows a widely diffuse increase in land-cover heterogeneity (Figure 10), suggesting that a deep reorganization of the floodplain is in progress. The evidence of ongoing vegetation decline (Table 1) seems to indicate that unless some actions are taken to mitigate the dam impact, the ecosystem shift will be unavoidable. The monitoring of the consequences of the dam on vegetation could guide the management policy of the hydropower plant addressing the recovery of this ecosystem, which is populated by a huge variety of vegetation species that reach more than 500 years of life (Schöngart et al., 2005; de Resende et al., 2020).

5 Conclusion

This study provides an operative framework for the evaluation of the impact of river regulation on floodplain vegetation based on the assessment of vegetation indices changes, hydrological alterations, and the modification of the forest gross primary production. The GFHR data was fundamental to study the extreme cloudy tropical area of the Amazon basin. The high spatial and temporal resolution analysis of floodplain forest allowed for the detection of modifications of vegetation behavior in terms of both inter- and intra-annual variability, even along the narrow aquatic-terrestrial transitional zone. The analysis of vegetation indices, not only in terms of variation of the annual mean of vegetation index, but also about the magnitude of the change and variation in phenology (amplitude of oscillation), guided the detection of vegetation species transitions. Our results suggest a deep reorganization in species populating the floodplain of Uatumã, in favor of a terrestrialization of the forest community. The study of hydrological alterations that affect the region with vegetation changes disentangled the role of the dam in forest alteration. In summary, the forest GPP analysis revealed that vegetation changes along the Uatumã are associated with a dramatic change in the floodplain primary production with possible consequences for the river carbon cycle.

Our approach is based on the identification and analysis of regions where vegetation changes are concentrated rather than a study of the average behavior of the entire floodplain, allowing very accurate identification of the most degraded or threatened area. The extreme heterogeneity of the forest ecosystems populating the tropical floodplain makes it difficult to generalize what is the response of these ecosystems to alterations in the hydrological regime. At the same time, the increasing number of dams under construction in the Neotropics makes urgent the availability of more accurate procedures for monitoring impacts. Our framework is a practical tool that could be potentially applied to map and monitor floodplain forests, guiding the assessment of the vegetation status and the identification of threatened areas.

Data Availability Statement

The original contributions presented in the study are included in the article/Supplementary Material, further inquiries can be directed to the corresponding author.

Author Contributions

LS, AM-M, EI-V, AS, CC contributed to conceptualization; LS, AM-M, EI-V contributed to methodology and software; LS, AS, CC contributed to investigation work; LS contributed to visualization, data curation, formal analysis, validation and writing—original draft; AM-M, EI-V, AS, CC contributed to review and editing; NC contributed to computing resources; AS, CC contributed to supervision. All authors approved the submitted version.


LS was supported by the Joint Projects grant funded by Compagnia di San Paolo Fundation. This research was partly funded by the ERC under the ERC-SyG-2019 USMILE project (grant agreement 855187).

Conflict of Interest

Author NC was supported by the company Google, Inc.,

The remaining authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Publisher’s Note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.


Credit for base map in Figure 1A–C, Figure 8 and Supplementary Figure S3–S8: Esri, DigitalGlobe, GeoEye, i-cubed, USDA FSA, USGS, AEX, Getmapping, Aerogrid, IGN, IGP, swisstopo, and the GIS User Community.

Supplementary Material

The Supplementary Material for this article can be found online at:


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Keywords: tropical riparian vegetation, floodplain monitoring, regulated rivers, satellite image analysis, dam regulation, vegetation indeces, gross primary production

Citation: Salerno L, Moreno-Martínez Á, Izquierdo-Verdiguier E, Clinton N, Siviglia A and Camporeale C (2022) Satellite Analyses Unravel the Multi-Decadal Impact of Dam Management on Tropical Floodplain Vegetation. Front. Environ. Sci. 10:871530. doi: 10.3389/fenvs.2022.871530

Received: 08 February 2022; Accepted: 18 March 2022;
Published: 10 May 2022.

Edited by:

Edoardo Daly, Monash University, Australia

Reviewed by:

Neil Sims, Commonwealth Scientific and Industrial Research Organisation (CSIRO), Australia
Alban Kuriqi, Universidade de Lisboa, Portugal

Copyright © 2022 Salerno, Moreno-Martínez, Izquierdo-Verdiguier, Clinton, Siviglia and Camporeale. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Luca Salerno,